Hydrous Melting

Hydrous Melting is a geochemical process in the context of partial melting whereby the presence of water or other volatile components reduces the melting temperature of silicate minerals, thereby facilitating magma generation at lower temperatures compared to dry melting conditions.

464

Publications

44.2K

Citations

1.1K

Authors

434

Institutions

Publications per year

2017–2026

88

Authors

1.1K

  1. HB
    Harald Behrens

    Leibniz University Hannover, Germany

    12 publications · 1.2K citations

    11

    h-index

  2. TL
    T. L. Grove

    Massachusetts Institute of Technology, United States

    10 publications · 1.7K citations

    10

    h-index

  3. EO
    Eiji Ohtani

    Tohoku University, Japan

    9 publications · 471 citations

    9

    h-index

  4. BS
    Bruno Scaillet

    Centre National de la Recherche Scientifique, France

    8 publications · 819 citations

    8

    h-index

  5. DB
    Donald B. Dingwell

    Ludwig-Maximilians-Universität München, Germany

    7 publications · 969 citations

    7

    h-index

1–5 of 1.1K

Venues

  1. Contributions to Mineralogy and Petrology

    48 publications · 6.5K citations

    32

    h-index

  2. Earth and Planetary Science Letters

    36 publications · 4K citations

    30

    h-index

  3. Journal of Petrology

    31 publications · 4.5K citations

    26

    h-index

  4. Geochimica et Cosmochimica Acta

    32 publications · 2.5K citations

    25

    h-index

  5. Chemical Geology

    25 publications · 1.9K citations

    21

    h-index

1–5